Large impacts, past and future, of ozone‐depleting substances on Brewer‐Dobson circulation trends: a multimodel assessment

• Main Authors: Polvani, L. M., Wang, L., Ábalos Álvarez, Marta, Butchart, N., Chipperfield, M. P., Dameris, M., Deushi, M., Dhomse, S. S., Jöckel, P., Stone, K. A.
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Geophysical Union 2019
• Subjects: 551.51; Brewer-Dobson circulation; Ozone-depleting substances; Age of air; Stratospheric circulation; Chemistry-climate models; Física atmosférica; 2501 Ciencias de la Atmósfera; South Pole; South pole
• Online Access: https://hdl.handle.net/20.500.14352/108238; https://doi.org/10.1029/2018jd029516

Atraccion de Talento de la Comunidad de Madrid (2016-T2/AMB-1405) Project STEADY (CGL2017-83198-R) Artículo firmado por 15 autores. Substantial increases in the atmospheric concentration of well-mixed greenhouse gases (notably CO_(2)), such as those projected to occur by the end of the 21st century under large radiative forcing scenarios, have long been known to cause an acceleration of the Brewer-Dobson circulation (BDC) in climate models. More recently, however, several single-model studies have proposed that ozone-depleting substances might also be important drivers of BDC trends. As these studies were conducted with different forcings over different periods, it is difficult to combine them to obtain a robust quantitative picture of the relative importance of ozone-depleting substances as drivers of BDC trends. To this end, we here analyze—over identical past and future periods—the output from 20 similarly forced models, gathered from two recent chemistry-climate modeling intercomparison projects. Our multimodel analysis reveals that ozone-depleting substances are responsible for more than half of the modeled BDC trends in the two decades 1980–2000.We also find that, as a consequence of the Montreal Protocol, decreasing concentrations of ozone-depleting substances in coming decades will strongly decelerate the BDC until the year 2080, reducing the age-of-air trends by more than half, and will thus substantially mitigate the impact of increasing CO_(2). As ozone-depleting substances impact BDC trends, primarily, via the depletion/recovery of stratospheric ozone over the South Pole, they impart seasonal and hemispheric asymmetries to the trends which may offer opportunities for detection in coming decades. Fudan University National Natural Science Foundation of China (NSFC) Comunidad de Madrid Ministerio de Economía, Industria y Competitividad (España) Met Office Hadley Centre Programme - BEIS Met Office Hadley Centre Programme - Defra European Commission NZ Governments Strategic Science ...